2025-03-20T16:00:00Z 2025-03-20T16:00:00Z 2025-03-21T16:00:00Z false Glockner Range Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Gurgler Range Central Stubai Alps Northern Zillertal Alps Venediger Range Lasörling Range Gröden Dolomites Lüsner Mountains Sexten Dolomites Upper Ahr Valley Southern Zillertal Alps Pfitsch Southern Sesvenna Group Schnals Ridge Northern Sesvenna Group Saldurn-Mastaun Ridge Hirzer Range Mount Saint Jakob Range Western Pfunderer Mountains Eastern Pfunderer Mountains Langtaufers Ratschings Durreck Range Rieserferner Mountains Southern Stubai Alps Western Deferegger Alps Ortler Range Ulten Valley Planeil Mountains Prags Dolomites Upper Passeier Valley Texel Mountains low 2200 all_day moderate 2200 all_day persistent_weak_layers 2200 W NE N E NW all_day poor some 2 slab wet_snow 2400 W SE SW E S all_day very_poor few 2 loose Weak layers in the old snowpack represent the main danger. Slight increase in danger of wet avalanches in the course of the day. Shady slopes: Weak layers in the old snowpack can still be released in some places by individual winter sport participants. The avalanche prone locations are to be found in particular on steep, little used slopes above approximately 2200 m. Individual avalanche prone locations are to be found also on sunny slopes in high Alpine regions. Mostly avalanches are medium-sized. In isolated cases avalanches can also release deeper layers of the snowpack and reach large size. The avalanche prone locations are barely recognisable, even to the trained eye. The current avalanche situation calls for meticulous route selection. Sunny slopes: As a consequence of warming during the day and the solar radiation, the likelihood of wet loose snow avalanches being released will increase a little. On extremely steep sunny slopes individual small and, in isolated cases, medium-sized natural avalanches are possible from the middle of the day. The new snow and wind slabs of last week are lying on the unfavourable surface of an old snowpack in particular on shady slopes at elevated altitudes. Avalanche prone weak layers exist in the old snowpack especially on little used shady slopes. The somewhat older wind slabs are now only very rarely prone to triggering. Sunny slopes: The snowpack will be in most cases well bonded. As a consequence of low temperatures a crust will form on the surface during the course of the night. The solar radiation will give rise as the day progresses to increasing moistening of the snowpack on steep sunny slopes. Below the tree line only a little snow is now lying. Weakly bonded old snow and wet snow require caution. The surface of the snowpack will cool hardly at all during the overcast night and will soften earlier than the day before. steady 2025-03-21T16:00:00Z 2025-03-22T16:00:00Z 2025-03-21 DP5 DP10 2025-03-20T16:00:00Z 2025-03-20T16:00:00Z 2025-03-21T16:00:00Z false Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps Eastern Karwendel Mountains Central Kitzbühel Alps Western Kitzbühel Alps low all_day wet_snow S W SE SW E all_day very_poor few 2 loose Slight increase in danger of wet avalanches in the course of the day. As a consequence of warming during the day and the solar radiation, the likelihood of wet loose snow avalanches being released will increase a little. On extremely steep sunny slopes individual small and, in isolated cases, medium-sized natural wet avalanches are possible from the middle of the day. This applies in particular in the regions with a lot of snow. Shady slopes: The snowpack is largely stable; its surface consists of loosely bonded snow. This applies in particular above approximately 2200 m. The somewhat older wind slabs have bonded well with the old snowpack. Sunny slopes: The snowpack will be in most cases well bonded. As a consequence of low temperatures and low relative humidity a crust will form on the surface during the course of the night. The solar radiation will give rise as the day progresses to increasing softening of the snowpack on steep sunny slopes. Below the tree line only a little snow is now lying. The surface of the snowpack will cool hardly at all during the overcast night. The weather conditions will give rise to increasing softening of the snowpack. This also applies at intermediate and high altitudes. The wind will be moderate to strong in particular in the regions exposed to the foehn wind. increasing 2025-03-21T16:00:00Z 2025-03-22T16:00:00Z 2025-03-21 DP10 2025-03-20T16:00:00Z 2025-03-20T16:00:00Z 2025-03-21T16:00:00Z false Eastern Lechtal Alps Ammergau Alps Kauner Ridge Weißkugel Range Western Verwall Mountains Eastern Verwall Mountains Silvretta Allgäu Alps Samnaun Mountains Mieming Mountains Western Tuxer Alps Eastern Tuxer Alps Western Lechtal Alps Kalkkögel Glockturm Range Central Lechtal Alps Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Western Karwendel Mountains low all_day wet_snow S W SE SW E all_day very_poor few 1 loose Slight increase in danger of wet avalanches in the course of the day. As a consequence of warming during the day and the solar radiation, the likelihood of wet loose snow avalanches being released will increase a little. On extremely steep sunny slopes individual mostly small natural wet avalanches are possible from the middle of the day. Individual avalanche prone locations for dry avalanches are to be found on extremely steep shady slopes at elevated altitudes, in particular adjacent to ridgelines. In regions exposed to the foehn wind these avalanche prone locations are a little more prevalent. Sunny slopes: The snowpack will be in most cases well bonded. As a consequence of low temperatures and low relative humidity a crust will form on the surface during the course of the night. Sunshine and high temperatures will give rise as the day progresses to increasing softening of the snowpack. Below the tree line only a little snow is now lying. Shady slopes: As a consequence of a moderate southerly foehn wind, clearly visible wind slabs will form in the regions exposed to the foehn wind. They are in isolated cases prone to triggering on shady slopes at elevated altitudes. Faceted weak layers exist deeper in the old snowpack on little used shady slopes. The surface of the snowpack will cool hardly at all during the overcast night. The weather conditions will give rise to increasing softening of the snowpack. This also applies at intermediate and high altitudes. The wind will be moderate to strong in particular in the regions exposed to the foehn wind. Fresh wind slabs in the high Alpine regions. increasing 2025-03-21T16:00:00Z 2025-03-22T16:00:00Z 2025-03-21 DP10 DP6